欧美宾夕法尼亚地区晚石炭世改良的扁虫类和贝壳纲的分带

J. Schneider, F. Scholze, A. Ross, B. M. Blake, S. Lucas
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引用次数: 8

摘要

摘要在欧洲美洲古热带陆-海混合剖面和纯大陆剖面的生物地层学研究中,新定义或改进了9个昆虫带和8个甲壳纲带。这些带涵盖了从早宾夕法尼亚(巴什基良中期)到早二叠纪(早亚塞利亚)的欧亚生物省的时间间隔。通过在海相-大陆混合剖面中常见的带有牙形刺的昆虫和/或贝壳类动物,以及迄今为止可获得的可靠的伴生火山岩的放射性同位素年龄,它们尽可能地与海洋标准全球年表相联系。这种昆虫和甲壳纲的分带是一种替代工具,以建立大型植物生物地层学的宾夕法尼亚。与后者相比,只有昆虫或贝壳类动物的单一标本,即使比植物遗骸更罕见,也可以用类似的高时间分辨率进行生物地层测年。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Improved blattoid insect and conchostracan zonation for the Late Carboniferous, Pennsylvanian, of Euramerica
Abstract For the biostratigraphy of mixed continental-marine and purely continental sections in the palaeotropical belt of Euramerica, 9 insect and 8 conchostracan zones are newly defined or improved. These zones encompass the time interval from the Early Pennsylvanian (middle Bashkirian) up into the early Permian (early Asselian) of the Euramercian biotic province. They are linked as much as possible to the marine Standard Global Chronostrigraphic Scale by common occurrences of insects and/or conchostracans with conodonts in mixed marine-continental sections as well as by the thus far available and reliable radioisotopic ages of associated volcanic rocks. This insect and conchostracan zonation is an alternative tool to the well-established macro-plant biostratigraphy of the Pennsylvanian. In contrast to the latter, only single specimens of insects or conchostracans, even if more rare than plant remains, allow biostratigraphic dating with a similar high temporal resolution.
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